泰国三机场高铁列控系统方案研究

对泰国三机场高铁项目的列控系统选择要求进行分析,提出列控系统方案并进行综合比选,最后提出泰国三机场高铁项目的列控系统推荐方案,研究成果可以为海外项目列控系统方案选择提供一定的参考。     

重载铁路四线高墩连续梁桥的设计

神瓦(神木—瓦塘)铁路冯家川车站大桥为重载铁路四线桥,主桥采用4线(65+100+65)m连续梁,最大墩高85 m.桥上线间距大,上下部结构横向尺寸较大,利用有限元分析软件BSAS,MIDAS/FEA对结构受力进行了计算分析.结果表明:在主梁梁高相同的情况下,采用单箱三室截面能更好地减小主应力,采用单箱双室截面增加腹板厚度对主应力的改善有限;多线桥桥墩横向尺寸较大,空心截面设置纵肋板能很好地提高高墩的局部稳定性;主梁及桥墩各项计算指标均满足规范要求.     

基于分段单孔反演的隧址区多断层地应力分布特征

目前，针对具有多个原位地应力测试钻孔的隧址区初始地应力场反演，往往一次性将全部实测值用以计算值的回归反分析，没有考虑到隧道纵向长度远超其他方向且钻孔分布较远的特点，单个钻孔表征的临近区域地应力分布特征或反演精度被其余钻孔实测值“拉低”，导致整体反演结果容易陷入局部优解。依托拉林铁路桑珠岭隧道、叙毕铁路斑竹林隧道、沿江高速火山隧道、木寨岭公路隧道等工程，采用多元线性回归法结合最小二乘法寻优准则，分析了隧址区仅有单个钻孔反演精度较高的原因，提出了对具有多个钻孔的隧址区分段并分别进行单钻孔回归反演的新方法。在此基础上，重点讨论了木寨岭公路隧道断层破碎带区域地应力分布特征。结果表明：分段单孔反演较多孔反演进一步提高了反演精度；地应力的分布在断层前后呈现出先急剧增大后急剧减小的特征；除自重应力与埋深存在一定关联外，两项水平主应力随断层间距或厚度的增大突变性加剧；断层之间间距、断层倾角、断层厚度均是影响地应力方向偏转大小的重要因素，断层之间间距或断层倾角越小、断层越厚，地应力方向偏转越显著。     

高桩码头纵梁维修加固方法及对比

20世纪70～80年代修建的高桩码头由于长期处于氯盐侵蚀的环境中,码头浪溅区梁板钢筋容易发生锈蚀膨胀,进而引起混凝土纵向开裂、脱落。为保证码头结构安全需要对此类型的梁进行维修加固,基于实际码头维修加固工程对加大梁截面和粘贴碳纤维布两种维修加固方法进行介绍,从应用范围、施工效率、质量及成本4个方面对两种方法进行对比分析。结果表明,加大截面法比粘贴碳纤维布法的适用范围更广泛,但在施工效率、成本、施工难易及质量可控性等方面,粘贴碳纤维布法具有明显优势。     

半约束模型试验--一种验证随浪和斜浪中波浪力计算的手段

本文采用半约束模型试验技术，对一条高速船在规则波中随浪和斜浪工况进行了流体动力系列试验，以探讨航运的安全性，验证作用于船体上波浪力的估算方法。对每次试验，以波动方程的形式采用数值估算方法确定环绕船模的波浪运动的时间历程。并用同样的方法从测量数据中提取垂荡和纵摇与模型测量运动，一阶波导纵荡、横荡作用力和首摇力矩。因此合理比较理论计算的波浪力与力矩的时间历程成为可能。这表明SSPA海事动力学的研究所(MDL)模型试验设施可以提供高质量的测量，与所述计算方法结合起来可用来验证理论计算和建立半经验方法。     

特殊条件下的真空预压密封技术

结合广州港南沙港区二期工程软基处理工程实例,针对在局部有抛石地段的软土采取真空预压方法加固时传统的挖密封沟和施打淤泥搅拌墙技术存在相当大困难的情况,提出了在有抛石地段采取高压旋喷桩密封技术。实测结果表明,采取该技术密封效果良好,真空度能达到设计要求。与堆载方案相比,采取本技术经济效益良好,具有较好的推广价值。     

Fluxes of dissolved inorganic carbon in three estuarine systems of the Cantabrian Sea (north of Spain)

The diffusive and in situ fluxes of dissolved inorganic carbon (DIC) and total alkalinity (TA) have been measured and an estimation has been made of the water–atmosphere fluxes of CO₂ in three estuarine systems of the Cantabrian Sea during the spring of 1998. Each of these systems undergoes a different anthropogenic influence. The diffusive fluxes of dissolved inorganic carbon and total alkalinity obtained present values ranging between 0.54–2.65 and 0.0–2.4 mmol m⁻² day⁻¹, respectively. These ranges are in agreement with those of other coastal systems. The in situ fluxes are high and extremely variable (35–284 mmol TA m⁻² day⁻¹, 43–554 mmol DIC m⁻² day⁻¹ and 22–261 mmol dissolved oxygen (DO) m⁻² day⁻¹), because the systems studied are very heterogeneous. The values of the ratio of the in situ fluxes of TA and DIC show on average that the rate of dissolution of CaCO₃ is 0.37 times that of organic carbon oxidation. Equally, the interval of variation of the relationship between the benthic fluxes of inorganic carbon and oxygen (F_DIC/F_DO) is very wide (0.3–13.9), which demonstrates the different contributions made by the processes of aerobic and anaerobic degradation of the organic matter, as well as by the dissolution–precipitation of CaCO₃. The water–atmosphere fluxes of CO₂ present a clear dependence on the salinity. The brackish water of these systems (salinity<20), where maximum fluxes of 989 mmol m⁻² day⁻¹ have been estimated, act as a source of CO₂ to the atmosphere. The more saline zones of the estuary (salinity>30) act as a sink of CO₂, with fluxes between −5 and −10 mmol m⁻² day⁻¹.     

牵引网微机保护整定的探讨

通过对牵引网负荷电流、短路电流中的谐波含量的分析和存在的谐波含量的不同点,利用两种电流中的综合谐波含量作为控制量,可以大大提高牵引网距离保护、高阻接地保护躲过牵引重负荷,再生负荷,启动电流及励磁涌流的能力,对于保护整定,通过探讨提出了整定原则和方法。     

生活小区管道直饮水的工艺及经济分析

分析了生活小区管道直饮水的净水工艺,对工艺流程各单元的原理和作用进行了阐述,并进行了经济分析,和桶装直饮水比较,管道直饮水的价格较低,表明生活小区管道直饮水系统有较大的发展空间。     

Organic carbon budget for the Gulf of Bothnia

We calculated input of organic carbon to the unproductive, brackish water basin of the Gulf of Bothnia from rivers, point sources and the atmosphere. We also calculated the net exchange of organic carbon between the Gulf of Bothnia and the adjacent marine system, the Baltic Proper. We compared the input with sinks for organic carbon; permanent incorporation in sediments and mineralization and subsequent evasion of CO₂ to the atmosphere. The major fluxes were riverine input (1500 Gg C year^− 1), exchange with the Baltic Proper (depending on which of several possible DOC concentration differences between the basins that was used in the calculation, the flux varied between an outflow of 466 and an input of 950 Gg C year^− 1), sediment burial (1100 Gg C year^− 1) and evasion to the atmosphere (3610 Gg C year^− 1). The largest single net flux was the emission of CO₂ to the atmosphere, mainly caused by bacterial mineralization of organic carbon. Input and output did not match in our budget which we ascribe uncertainties in the calculation of the exchange of organic carbon between the Gulf of Bothnia and the Baltic Proper, and the fact that CO₂ emission, which in our calculation represented 1 year (2002) may have been overestimated in comparison with long-term means. We conclude that net heterotrophy of the Gulf of Bothnia was due to input of organic carbon from both the catchment and from the Baltic Proper and that the future degree of net heterotrophy will be sensible to both catchment export of organic carbon and to the ongoing eutrophication of the Baltic Proper.